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Crystallographical analysis of shear bands initiation and propagation in pure metals
Ph. Dubois, C. Rey
To cite this version:
Ph. Dubois, C. Rey. Crystallographical analysis of shear bands initiation and propagation in pure metals. Revue de Physique Appliquée, Société française de physique / EDP, 1988, 23 (4), pp.696-696.
�10.1051/rphysap:01988002304069600�. �jpa-00245844�
696
CRYSTALLOGRAPHICAL ANALYSIS OF SHEAR BANDS INITIATION AND PROPAGATION IN PURE METALS
Ph. DUBOIS and C. REY
LPMTM, Université PARIS-NORD - Av. J.B. Clément 93430 - VILLETANEUSE
Revue
Phys. Appl.
23(1988)
696 AVRIL1988,
Our purpose was to determine conditions of shear bands initiation and propagation in pure copper
single or polycrystals sollicited by tensile load and rolling.
Tensile tests were carried out "in situ" on single crystal oriented for double slip, thanks to a SEM.
So we were able to determine the crystallographi-
cal nature of shear planes for various tensile axis orientation. Four orientations closed to
|001|, |-1,1,3|, |-1,1,2|
and|-1,1,1|
wereinvestigated. In all cases shear banding occured
in the necking area after a mean strain of about 55%. "In situ" observations pointed out that the localization mode was always caracterized by shearing in a very thin and planar band which width increased with increasing strain.
We had compared our experimental results to the prediction of the theoretical model developped by
Pierce
Ill
for rigid plastic materials. Founded upon Biot(2I,
Hill andHutchinson 131
and Pierce Asaro and Needleman|4|
works.-, It was assumed thatcrystal plasticity was rate independent, governed by Schmid’s law, moreover the crystal was oriented
in double ship deformation for tensile loading.
For such a double orientation, a thin band of intense shearing limited by two nearly parallel planes grew in the crystal (fig.1). The transfor- mation gradient rate F was supposed to show an abrupt change of value in the thin band compared
to the bulk one.
According to different authors, the discontinuity
must be of the form :
where G and N were the shearing vector and the
unit normal to the band. Traction rates must be continuous across the shear planes, so one must
have :
where S was the nominal stress tensor.
The misfit between experimental observations and theoretical predictions about crystallographical
orientations of shear planes led us to introduce
in the model some other parameters in order to take into account :
- the tensile test direction
- the stress field induce by the neck
- conditions on the strain field compa- tibility.
Fig.1 Shear-band mode for tensile loa- ding.
By these formulation we defined "potential shear systems" and are studying some criterions in order to determine the more favorable systems.
In polycrystals case, strained by rolling, fidu-
cial grids were set down on the longitudinal section, in order to point out the displacement
induced by shear bands and to analyse the inter- action between shear bands and grain boundaries. A 1 MM2 square grid with 5 vm mesh size and an
average 0.5 um grid line was obtained by a photo-
resist technique, using the beam of a SEM. Our observations, pointed out that (Fig.2) :
- macroscopical shear bands were constituted of
microscopical ones
- shearing intensity was proportional to the
number of microscopical bands activated inside
macroscopical ones
- strain increased by elongation of initial shear bands and nucleation of new bands in the
vicinity of initial ones.
Previous works on rolled polycrystals have reported that shear bands appeared inside somme especially oriented grains. With intend to carac-
terize the conditions of initiation and propa- gation of such bands, experiments on special
oriented bicrystals have been undertaken.
REFERENCES
1 D. PEIRCE J. Mech. Phys. Solids 31 (1983) 133.
2 M.A. BIOT "Mechanics of Incremental Deforma-
tions", edited by Willey (1965).
3 R. HILL and J.W.. HUTCHINSON J. Mech. Phys.
Solids, 23 (1975) 239.
4 D. PEIRCE et al Acta Met. 30 (1982) 1087.
Fig.2 Propagation of shear band in rol- led polycrystals.
- Initial bands,...new bands.
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/rphysap:01988002304069600